簡介:"礦物硫化物及硫鹽銻銀礦Dyscrasite Sulfides and SulfosaltsDyscrasite is the primary ore mineral of antimony and silver, distinctive for its high density.Pyramidal dyscrasite crystals are exceptionally rare and are usually found in massive, sheety or granular habits. dyscrasite is soluble in nitric acid and produces Sb2O3 sediments.Named by F.S. Beudant in 1832.主要由銻和銀所組成,為重要的含銻和含銀礦物,比重大為其特徵之一。 錐狀晶體甚為少見,通常外觀多呈塊狀、片狀或粒狀。此種礦物可被硝酸所溶解,並產生三氧化二銻的白色沉澱。 銻銀礦係由F. S. Beudant於1832年所命名。"